Voi Safari Lodge stands high above the town of Voi overlooking a vast expanse of the African Bush. Just 160km from Mombasa City, the lodge is within easy access to both the eastern and western portions of the vast Tsavo ecosystem - one of the World's Largest Game Parks. Strategically situated, overlooking three waterholes, guests can simply watch the herds of wild animals roam beneath as they enjoy the ever-changing panorama of African wilderness unfold.

Kenya hotels and accommodation Amongst the wide range of Kenya hotels, some make the ideal Kenya safari destination. Choose a safari lodge, safari hotel, bush camp, luxury lodge, safari camp, tented camp or bush lodge. National park accommodation usually takes the form of a traditional safari lodge or tented camp, but numerous other options exist on the park boundaries. Luxury lodges and luxury camp options are also offered in the private wildlife conservancies.

Location Tsavo East National Park is easily accessible by air and road, and is approximately 160 kilometers from Mombasa, and 326 kilometers from Nairobi. Voi Safari Lodge, built in 1969, is strategically situated in one of the World's Largest Game Park - the Tsavo East National Park. Voi Safari Lodge stands high above the town of Voi overlooking a vast expanse of the African Bush. The lodge is easily reached by car from Voi Town (on the main Mombasa-Nairobi Highway). There is an airstrip 4 km from the lodge.

The Background Theatre of the wild The joint mass of Tsavo West and Tsavo East National Parks forms one of the largest national parks in the world and covers a massive 4% of Kenya's total land area.

Tsavo East, one of the last great wilderness landscapes on Earth, offers a vast arena of parched scrub and heat-shimmering bush, which is washed by the azure waters and emerald-fringed meanderings of the Galana River, guarded by the limitless lava reaches of the Yatta Plateau and patrolled by some of the largest elephant herds in the world.

Tsavo West, land of lions and lava, is painted on a sprawling canvas of endless skies, emerald hills, liquid lava flows, palm-fringed rivers, teeming wildlife and sparkling oases, where rafts of hippo wallow, snort and blow in the crystal clear melt waters of Mount Kilimanjaro.

Kenya's largest National Park supports all the members of the ‘Big Five' as well as the country's largest elephant population. Tsavo achieved notoriety in the 1900's when ‘the Man-eaters of Tsavo', a pair of rogue man-eating lions, preyed gruesomely on the builders of the Uganda Railway. Today the Park is more famous for the numerous prides of mane-less lion that patrol the plains and police the herbivore herds. Wildlife highlights: elephant, lion, hippo, rhino, zebra, hartebeest, lesser kudu, eland, waterbuck, Grant's gazelle, impala, gerenuk, giraffe, dik dik and klipspringer. Birds: 600 recorded species.

Accommodation The lodge offers 53 standard ensuite rooms.

Dining and bars The lodge has a large central dining room and two bars. The pool terrace offers magnificent views across the plains and looks directly down on three waterholes. The lodge also offers its own photo-hide, which is reached by a tunnel leading direct to the nearest waterhole.

Child-friendly The lodge welcomes children and additional beds can be provided.

What to see and doAruba Dam Aruba Dam is an 85-hectare man-made dam built by the Parks authorities in 1952 to staunch the waters of the seasonal Voi River, which flows down from the Taita Hills in the southwest. It usually holds water throughout the year and is frequented by huge numbers of ibis, many grey heron and a kaleidoscope of other water birds. It is also part of the territory of a large pride of lion, which can often be seen in the dam's vicinity.

Kanderi Swamp The Kanderi Swamp lies near Voi Gate and during the dry months provides one of only two drinking areas in Tsavo East, thus attracting large herds of buffalo, impala and antelopes as well as yellow baboons and lion.

Mudanda Rock Kenya's answer to Ayer's Rock of Australia is called Mudanda Rock, a massive 1.5km whale-backed rock which rears out of the shrub between Manyani Gate and Voi and is famous for its photo-opportunities, offering marvellous light, panoramic vistas and an excellent chance of prime wildlife shots. It is also an excellent vantage point from which to look down on the natural dam below, which can at times attract hundreds of elephant. This area is also known as a favourite leopard haunt, though daytime sightings are rare.

The Galana River The Tsavo and Athi Rivers join above Lugard's Falls to form the Galana River, which then flows down to the Indian Ocean. A major feature of the park, the serpentine reaches of this river are fringed by riverine forests dominated by Acacia elatior, the Doum Palm Hyphaene compressa and the shrub Suaeda monoica.

Lugard's Falls Named after Britain's first proconsul in East Africa, Captain (later Lord) Lugard, the falls are better described as rapids than falls progressing from foaming cataracts to narrow cascades that gouge deep into the gneiss bedrock creating fantastic shapes that have been surreally rounded by thousands of years of rushing water.

Mighty when in full spate, the falls gush through a small fissure, narrow enough for the foolhardy to leap across, before plunging to the pool below, where massive crocodiles bask motionless in the sun. There is a parking area at the falls and visitors either climb around the bizarrely eroded rocks or walk down the river to view the rapids. 1km east of the falls another short diversion takes you to Crocodile Point where hippos and buffalo wallow and zip-jawed crocodile grin.

The Yatta Plateau, an ancient valley frozen in time The Yatta plateau is a ridge or tongue of lava about 300km long and a maximum of 10km wide, which forms a seemingly never-ending backdrop to Tsavo East. One of the longest lava flows in the world, the Yatta affords fabulous views across the rolling reaches of the Park, is an ornithological paradise and makes a peerless sundowner or picnic spot. It is made up of a form of lava known as phonolite, which is between 11 and 13.6 million years old. Current thought suggests that the Yatta Plateau was formed when a stream of lava flowed across the land until it found its way into an ancient river valley. The lava then flowed down the valley; taking on the shape of its contours, until eventually it cooled and solidified. Thereafter the surrounding land was gradually lowered by erosion leaving the frozen river of lava standing up as a ridge.